Abstract
This article presents data on vertical methane fluxes in mesooligotrophic peatlands of the middle taiga subzone by the eddy covariance method. We have found a link between the methane emission rate and the changes in groundwater level (GWL) and soil temperature at a depth of 10–20 cm in seasonal dynamics. The total methane emission from April to October was 22.4 g m−2; this value is higher than the values obtained by other authors in circumboreal peatland ecosystems.
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